Relative soil water content as a factor for wind erodibility in soils with different texture and aggregation
The soil water content is one of the main factors influencing the beginning of soil particle movement by the wind. Although, some authors studied the effect of soil water content on threshold wind velocity and have defined a value to prevent wind erosion, the critical relative soil water content (HR...
| Autores principales: | , , , , |
|---|---|
| Formato: | Artículo |
| Lenguaje: | Inglés |
| Publicado: |
Elsevier
2019
|
| Materias: | |
| Acceso en línea: | https://www.sciencedirect.com/science/article/pii/S1875963718302040 http://hdl.handle.net/20.500.12123/4543 https://doi.org/10.1016/j.aeolia.2019.02.001 |
Ejemplares similares: Relative soil water content as a factor for wind erodibility in soils with different texture and aggregation
- The impact of agriculture on soil texture due to wind erosion
- Soil dry aggregate stability and wind erodible fraction in a semiarid environment of Argentina
- RWEQ wind erosion predictions for variable soil roughness conditions
- Comparing adjacent cultivated and “virgin” soils in wind erosion affected environments can lead to errors in measuring soil degradation
- Comparison of organic versus mineral resource effects on short-term aggregate carbon and nitrogen dynamics in a sandy soil versus a fine textured soil
- PM10 emission, sandblasting efficiency and vertical entrainment during successive wind-erosion events: a wind-tunnel approach
